BAja California Ancient Marine Systems (BACAMS)


The former Turbidites Research Group at the University of Aberdeen initiated groundbreaking research, and BACAMS (Baja California Ancient Marine Systems) continues this legacy. The BACAMS project dedicates itself to advancing our comprehension of sedimentary processes and resulting deposits in submarine channel systems.

Since 2019, we are meticulously mapping the sedimentary architecture of several ancient slope channel systems to unravel their intricate complexities. We have started to explore and map areas that had never been studied by sedimentologist before because of its difficult access. Examining coarse-grained facies distribution has been central to our research, illuminating the dynamic interplay of bypass-dominated channel architecture. We are remapping contacts between channel belts and levees, the last characterized by thin-bedded architectures, utilizing vertical sequences as a crucial tool in identifying slope channel architectures. 

Our investigations have led to the discovery of new burnt tree trunks within stratigraphic units distinct from previous findings, adding a new dimension to interpretations on the role of the Chicxulub Impact Event.

Through the BACAMS project, we are not only expanding our understanding of ancient marine systems but also pioneering innovative insights into the geological history of the Baja California region.


A world marvel of coarse-grained slope channel complexes interbedded by mass transport complexes

Tree trunks in marine sequences with and without burnt evidences.